Basement and Regional Structure Along Strike of the Queen Charlotte Fault in the Context of Modern and Historical Earthquake Ruptures PublicDeposited

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Descriptions

The Queen Charlotte fault (QCF) is a dextral transform system located
offshore of southeastern Alaska and western Canada, accommodating ∼4.4 cm/yr of
relative motion between the Pacific and North American plates. Oblique convergence
along the fault increases southward, and how this convergence is accommodated is
still debated. Using seismic reflection data, we interpret offshore basement structure,
faulting, and stratigraphy to provide a geological context for two recent earthquakes,
an M[subscript w] 7.5 strike-slip event near Craig, Alaska, and an M[subscript w] 7.8 thrust event near Haida
Gwaii, Canada. We map downwarped Pacific oceanic crust near 54° N, between the
two rupture zones. Observed downwarping decreases north and south of 54° N, parallel
to the strike of the QCF. Bending of the Pacific plate here may have initiated with
increased convergence rates due to a plate motion change at ∼6 Ma. Tectonic reconstruction
implies convergence-driven Pacific plate flexure, beginning at 6 Ma south of
a 10° bend the QCF (which is currently at 53.2° N) and lasting until the plate translated
past the bend by ∼2 Ma. Normal-faulted approximately late Miocene sediment above
the deep flexural depression at 54° N, topped by relatively undeformed Pleistocene
and younger sediment, supports this model. Aftershocks of the Haida Gwaii event indicate
a normal-faulting stress regime, suggesting present-day plate flexure and underthrusting,
which is also consistent with reconstruction of past conditions. We thus
favor a Pacific plate underthrusting model to initiate flexure and accommodation
space for sediment loading. In addition, mapped structures indicate two possible fault
segment boundaries along the QCF at 53.2° N and at 56° N.